黑龙江省老柞山金矿床特征及找矿方向  

The features and prospecting direction of Laozhuoshan gold deposit,Heilongjiang Province

作　　者：王泉[1] 李碧乐[1] 李伟实 

机构地区：[1]吉林大学,吉林长春130061 [2]黑龙江省有色金属地质勘查研究总院,黑龙江哈尔滨150046

出　　处：《吉林地质》2006年第2期12-15,27,共5页Jilin Geology

摘　　要：老柞山金矿具多来源复合成因特点,产于佳木斯隆起内红卫中生代火山盆地边缘、前寒武纪花岗岩—绿岩带内,并有后期深成组分叠加。北西向、北西西向断裂带为控矿构造。本文通过讨论矿质来源、元素迁移富集等内容,指出进一步找矿方向。The Laozhuoshan gold deposit is characterized by polysources and compound genesis which occurs in the Precambrian granite-greenstone belt of the edge of Mesozoic Hongwei volcanic basin of Jiamusi doming and is reformed by later metallogenic materials from depth. The NW and NWW fault belts controlled the forming of the deposit. The authors pointed out the prospecting direction based on the discussion on the sources of the ore-forming materials, the migration and enrichment characteristics of elements.

关 键 词：花岗岩-绿岩带 多来源复合成矿 脉状金矿体 构造控矿 老柞山 

分 类 号：P618.51[天文地球—矿床学]